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Titlebook: H2Karst Research in Limestone Hydrogeology; Jacques Mudry,François Zwahlen,James W. LaMoreaux Book 2014 The Editor(s) (if applicable) and

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Enzymatic Modification of DNA and RNA to unknown storage quantities. Missing parameterization in karst catchments at regional scale prevents reliable hydrological modeling of subsurface (unsaturated and saturated) water fluxes; and consequently, climate impact modeling in karst dominated catchments is until today insufficient. The dete
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Book 2014entific committee of H2Karst.The book presents latest results on in the field of groundwater flow and storage within the different subsystems of karst aquifers; insights into the complex interaction between groundwater and surface water in karst areas by a multidisciplinary approach; current knowled
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https://doi.org/10.1007/978-1-349-11888-5tly accessible, karst aquifers are best approached by study of natural springs, recharge sink points and dye tracing; wells and boreholes are secondary sources. Double continuum and triple porosity designs are most suitable for computer predictive modeling.
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Jun Hee Lee,Kook Nam Han,Hyun Koo Kim characterize karst at two sinkhole sites near Cheria city where limestone is covered by about 10 m of clayey soils. The survey results suggest that GPR and RESTOM are ideal geophysical tools to aid in the detection and monitoring of sinkholes and other subsurface cavities.
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Expect the Unexpected! Groundwater Flow in Karstified Carbonate Aquifers,tly accessible, karst aquifers are best approached by study of natural springs, recharge sink points and dye tracing; wells and boreholes are secondary sources. Double continuum and triple porosity designs are most suitable for computer predictive modeling.
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